Outcomes and influencing factors of dental implants in fibula, iliac crest, and scapula free flaps: a retrospective case-control study.

PURPOSE: Reconstruction with vascularized bone grafts after ablative surgery and subsequent dental rehabilitation with implants is often challenging; however, it helps improve the patient's quality of life. This retrospective case-control study aimed to determine the implant survival/success rates in different vascularized bone grafts and potential risk factors. METHODS: Only patients who received implants in free vascularized bone grafts between 2012 and 2020 were included. The free flap donor sites were the fibula, iliac crest, and scapula. The prosthetic restoration had to be completed, and the observation period had to be over one year after implantation. Implant success was defined according to the Health Scale for Dental Implants criteria. RESULTS: Sixty-two patients with 227 implants were included. The implant survival rate was 86.3% after an average of 48.7 months. The causes of implant loss were peri-implantitis (n = 24), insufficient osseointegration (n = 1), removal due to tumor recurrence (n = 1), and osteoradionecrosis (n = 5). Of all implants, 52.4% were classified as successful, 19.8% as compromised, and 27.8% as failed. Removal of osteosynthesis material prior to or concurrent with implant placement resulted in significantly better implant success than material not removed (p = 0.035). Localization of the graft in the mandibular region was associated with a significantly better implant survival (p = 0.034) and success (p = 0.002), also a higher Karnofsky Performance Status Scale score with better implant survival (p = 0.014). CONCLUSION: Implants placed in vascularized grafts showed acceptable survival rates despite the potential risk factors often present in these patient groups. However, peri-implantitis remains a challenge.

Authigenic mineral phases as a driver of the upper-ocean iron cycle.

Iron is important in regulating the ocean carbon cycle1. Although several dissolved and particulate species participate in oceanic iron cycling, current understanding emphasizes the importance of complexation by organic ligands in stabilizing oceanic dissolved iron concentrations2-6. However, it is difficult to reconcile this view of ligands as a primary control on dissolved iron cycling with the observed size partitioning of dissolved iron species, inefficient dissolved iron regeneration at depth or the potential importance of authigenic iron phases in particulate iron observational datasets7-12. Here we present a new dissolved iron, ligand and particulate iron seasonal dataset from the Bermuda Atlantic Time-series Study (BATS) region. We find that upper-ocean dissolved iron dynamics were decoupled from those of ligands, which necessitates a process by which dissolved iron escapes ligand stabilization to generate a reservoir of authigenic iron particles that settle to depth. When this 'colloidal shunt' mechanism was implemented in a global-scale biogeochemical model, it reproduced both seasonal iron-cycle dynamics observations and independent global datasets when previous models failed13-15. Overall, we argue that the turnover of authigenic particulate iron phases must be considered alongside biological activity and ligands in controlling ocean-dissolved iron distributions and the coupling between dissolved and particulate iron pools.

Evaluation of the sense of taste and smell in patients with Neurofibromatosis Type 1.

OBJECTIVE: The objective of this study was to determine if patients with Neurofibromatosis Type 1 (NF1) have an impaired sense of smell or taste. Neurofibromin, the NF1gene protein product is ubiquitous in the body and is especially associated with the development of neurogenetic structures. Lately enlarged olfactory bulbs have been described in patients with NF1. Until now, there is no study to evaluate the sense of smell and taste in patients with NF1. METHOD: This study has been approved by the Hamburg Ethics committee. An evaluation of the sense of smell and taste was undertaken in 26 patients with NF1 using the Burghart Sniffin' Sticks. Three patients were excluded due to a prior infection with the Corona virus. As a control group the same examination was performed in healthy individuals (same sex/ same age as the NF1 patients) by the same examiner. RESULTS: The results show a normal sense of smell in patients with NF1. The morphologic finding of enlarged olfactory bulbs seem to have no functional equivalent. However, 8 out of 23 patients with NF1 had difficulties identifying at least one taste flavor. In total 9.8% of possible taste qualities were misidentified. In the healthy control group, all taste qualities were identified correctly. Considering each taste quality as separate case, a significant difference in the taste function was identified based on Fisher's exact test (p=0.003). CONCLUSION: The current study does not show a correlation between NF1 and an impaired sense of smell. Yet significant reduction in the sense of taste was found in the patients with NF1. Further research will have to be conducted to find the underlying causal pathways. CLINICAL RELEVANCE: NF1 is recently being acknowledged not only for its' macroscopic aesthetic and functional impairments, but also as a neurodevelopmental disorder. Evaluating the neural structures in regard to their function is a first step in understanding more about the disease.

A new surgical approach to treatment of bilateral syngnathia in a patient with popliteal pterygium-syndrome.

This case describes the treatment of syngnathia with a popliteal-pterygium syndrome. Although short-term successful surgical treatment has been described in literature, long-term follow up is essential, as the mouth opening limitations can be repetitively reoccurring. This requires new, individual treatment strategies as demonstrated in this case. A young patient is shown, who is successfully undergoing an alloplastic temporomandibular joint replacement to improve mouth opening, increasing the posterior airway space and facilitating the food intake.

Massive Transoral Bleeding from the Internal Carotid Artery in a Patient With Granulomatosis With Polyangiitis (Wegener).

BACKGROUND: In the oral and maxillofacial area, granulomatosis with polyangiitis (GPA) can lead to extended tissue destruction. CASE REPORT: This is a case report of a life-threatening local complication resulting from a large osseous defect in the cranial base with consecutive massive bleeding from the right internal carotid artery. Intraoperative examination and diagnostic imaging led to neuroradiological interventional treatment by embolization, and in neurosurgical and further reconstructive surgical treatment by the oral and maxillofacial surgeons. The purpose of this case report was to draw attention to the possibly life-threatening local complications of GPA and to discuss the importance of early intervention. CONCLUSION: As a prevention strategy, regular examinations including three-dimensional radiographic diagnostic imaging are important for the early detection of complications and the possible involvement of important structures.

Iron colloids dominate sedimentary supply to the ocean interior.

Dissolution of marine sediment is a key source of dissolved iron (Fe) that regulates the ocean carbon cycle. Currently, our prevailing understanding, encapsulated in ocean models, focuses on low-oxygen reductive supply mechanisms and neglects the emerging evidence from iron isotopes in seawater and sediment porewaters for additional nonreductive dissolution processes. Here, we combine measurements of Fe colloids and dissolved δ56Fe in shallow porewaters spanning the full depth of the South Atlantic Ocean to demonstrate that it is lithogenic colloid production that fuels sedimentary iron supply away from low-oxygen systems. Iron colloids are ubiquitous in these oxic ocean sediment porewaters and account for the lithogenic isotope signature of dissolved Fe (δ56Fe = +0.07 ± 0.07‰) within and between ocean basins. Isotope model experiments demonstrate that only lithogenic weathering in both oxic and nitrogenous zones, rather than precipitation or ligand complexation of reduced Fe species, can account for the production of these porewater Fe colloids. The broader covariance between colloidal Fe and organic carbon (OC) abundance suggests that sorption of OC may control the nanoscale stability of Fe minerals by inhibiting the loss of Fe(oxyhydr)oxides to more crystalline minerals in the sediment. Oxic ocean sediments can therefore generate a large exchangeable reservoir of organo-mineral Fe colloids at the sediment water interface (a "rusty source") that dominates the benthic supply of dissolved Fe to the ocean interior, alongside reductive supply pathways from shallower continental margins.